碳还原辅助消解-电感耦合等离子体发射光谱法测定锑矿石中的锑

Determination of Antimony in Antimony Ores Using Carbon Reduction-Assisted Digestion Coupled with Inductively Coupled Plasma Optical Emission Spectrometry

  • 摘要: 针对难溶锑酸盐矿物(如锑铁矿)在常规酸溶法中不易完全分解,导致锑测定结果偏低的问题,现有碱熔法、微波消解法虽有应用,但存在试剂干扰、依赖专用设备等局限。本文开发了一种基于原位碳还原机理的样品前处理方法。该方法采用酒石酸-氢氟酸-硝酸-硫酸混合酸体系,在高温条件下利用浓硫酸碳化酒石酸,原位生成强还原性的碳单质,将Sb(Ⅴ)高效还原为Sb(Ⅲ),从而抑制锑酸沉淀生成,实现了难溶锑酸盐矿物的完全溶解,确保了锑矿石中锑元素测定结果的准确性。通过优化,实验确定的最优参数为:采用1.0 mL 10%酒石酸为碳源的混合酸体系,在180℃温度下辅助消解锑矿物;并以10 mL浓硝酸作为提取酸,同时实现锑的提取与残余碳质的去除,采用电感耦合等离子体发射光谱法(ICP-OES)测定锑含量。方法精密度高(RSD为0.23% ~ 1.74%,检出限为17.7 μg/g,加标回收率在96.2% ~ 104.4%之间,符合《地质矿产实验室测试质量管理规范》(DZ/T 0130.3—2006)的要求。经锑矿石国家标准物质和实际样品验证,标准物质测定值与标准值一致,实际样品测定结果与常压密闭微波消解法吻合,表明方法准确可靠、实用性强。本方法在常压开放条件下消解,消除了对专用设备的依赖,结合ICP-OES测定,可满足大批量锑矿石样品的快速检测需求,即使对于锑含量高达40%的高品位样品,仍具备准确的检测能力。

     

    Abstract: Refractory antimonate minerals (e.g., tripuhyite) are difficult to decompose completely using conventional acid digestion methods, often leading to underestimated results in antimony determination. Although alkaline fusion and microwave digestion have been applied, these approaches may suffer from reagent interference or require specialized equipment. In this study, a novel sample pretreatment strategy based on an in situ carbon reduction mechanism was developed. The method employs a mixed acid system consisting of tartaric acid, hydrofluoric acid, nitric acid, and sulfuric acid. Under high-temperature conditions, concentrated sulfuric acid carbonizes tartaric acid to generate strongly reducing elemental carbon in situ, which efficiently reduces Sb(Ⅴ) to Sb(Ⅲ). This process suppresses the formation of antimonate precipitates and enables the complete dissolution of refractory antimonate minerals, thereby improving the accuracy of antimony determination in antimony ores. The optimized conditions involved the use of 1.0 mL of 10% tartaric acid as the carbon source in the mixed acid system, with assisted digestion at 180℃. Subsequently, 10 mL of concentrated nitric acid was used as the extraction acid to simultaneously extract antimony and remove residual carbonaceous material. The method exhibited a relative standard deviation (RSD) of less than 5% and a detection limit of 17.7 μg/g. Spike recoveries ranged from 96.2% to 104.4%, meeting the requirements of the Geology and Minerals Laboratory Testing Quality Management Standards (DZ/T 0130.3—2006). Validation using certified reference materials and real samples showed that the measured values for reference materials were consistent with certified values, while results for real samples agreed well with those obtained by the atmospheric closed-vessel microwave digestion method, demonstrating the accuracy and reliability of the proposed method. The digestion is carried out under atmospheric open conditions, eliminating the need for specialized equipment. When combined with ICP-OES determination, the method enables rapid analysis of large batches of antimony ore samples and remains accurate even for high-grade samples containing up to 40% antimony.

     

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